Macrodon sulcatus Weller 1906

Abstract

Macrodon sulcatus Weller, 1906 Original source Weller (1906): 450, pl. 2 figs 6–9. Type stratum and age “Glen Park Limestone”; Glen Park Formation, Kinderhookian, Mississippian, Carboniferous. Type locality “ Goetz’s lime quarry, just below Glen Park station on the St. Louis, Iron Mountain and Southern Railroad, about twenty-five miles south of St. Louis, in Jefferson County, Missouri ”, United States of America. Type material Williams (1931) indicated the syntypes (“cotypes”) to be stored at the Field Museum of Natural History, Chicago (FMNH UC 11335). Remarks First listed as Parallelodon by Moore (1928); further described and discussed by Williams (1931, 1943).

Authors 3

1. Julia C. Friedel

   University of Cologne

   Affiliation as printed

   Institute of Geology and Mineralogy, University of Cologne, Zülpicher Str. 49 a, 50674 Cologne, Germany

2. Thomas A. Neubauer Aachen Department of Earth and Environmental Sciences

   Ludwig-Maximilians-Universität München · Bavarian Natural History Collections · Naturalis Biodiversity Center · Bayerische Staatssammlung für Paläontologie und Geologie

   Affiliation as printed

   SNSB - Bavarian State Collection for Palaeontology and Geology, Richard-Wagner-Strasse 10, 80333 Munich, Germany. & Department of Earth and Environmental Sciences, Palaeontology & Geobiology, Ludwig-Maximilians-Universität München, Richard-Wagner-Str. 10, 80333 Munich, Germany. & Naturalis Biodiversity Center, Darwinweg 2, 2333 CR Leiden, The Netherlands

3. Michael R. W. Amler

   University of Cologne · Philipps University of Marburg

   Affiliation as printed

   Institute of Geology and Mineralogy, University of Cologne, Zülpicher Str. 49 a, 50674 Cologne, Germany. & Department of Geography, Philipps-Universität Marburg, Deutschhausstr. 10, 35032 Marburg, Germany